Wave Height Wind Force Calculator
Estimates significant sea wave height in meters from average wind speed in knots and wind fetch using a simple empirical relation for sailors.
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Wave height from wind force
Three things push wave height up: how hard the wind blows, the fetch (open distance over water) and how long it lasts. What most forecasts quote is the significant wave height H₁/₃, the mean of the highest one-third of waves, which lands close to what a trained observer would call out by eye. The Beaufort scale ties wind to sea state. Force 6 (39-49 km/h) gives 2.5-4 m waves; force 8 (62-74 km/h, gale) gives 4-5.5 m; force 10 (89-102 km/h, storm) gives 7-9 m. Feed in a 20-knot wind over 150 NM of fetch and a fully developed sea settles around 2 m H₁/₃.
Applications
It shows up in maritime navigation and ship routing (Marinha do Brasil issues forecasts in METMAR), in big-wave surfing (North Shore in Hawaii reaches 6-10 m in winter, while Nazaré in Portugal sees 20-30 m faces), in oceanographic models such as SWAN and WAVEWATCH III run by INPE, in offshore platform design, and in figuring out operational windows for transferring crew onto wind turbines.
FAQ
What is fetch? It's the unbroken stretch of open water the wind travels across. A longer fetch means more energy handed to the sea surface, until the water reaches a fully developed state.
How does H₁/₃ relate to the maximum wave? In a typical sea, the biggest wave you'd expect over three hours runs about 1.85 times H₁/₃, and over 24 hours it can climb to roughly 2.1 times.
Why two waves of the same height feel different? It comes down to period and steepness. A long-period swell (14-20 s) rolls through gently, whereas a short, steep wind wave (4-6 s) breaks hard and puts small craft at much greater risk.
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The results provided by this tool are for general informational and educational purposes only and do not constitute professional, financial, medical, legal, tax or accounting advice. Always confirm important decisions with a qualified professional and official sources.